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  2. Geography of the Bahamas - Wikipedia

    en.wikipedia.org/wiki/Geography_of_the_Bahamas

    The Bahamas is expected to be highly affected by sea level rise because at least 80% of the total land is below 10 meters elevation. [19] [20] As a small island developing state, the Bahamas is vulnerable to escalating disease outbreaks, and climate change could affect the seasonality of outbreaks and transmission of disease. [21]

  3. 1932 Abaco hurricane - Wikipedia

    en.wikipedia.org/wiki/1932_Abaco_hurricane

    It was known as the Great Abaco hurricane [nb 1] or the 1932 Bahamas hurricane, after the site of its worst effects, which it hit at peak intensity. Though large and powerful, it impacted few areas other than islands.

  4. Sea of Abaco - Wikipedia

    en.wikipedia.org/wiki/Sea_of_Abaco

    The Sea of Abaco (sometimes Abaco Sound), located in The Bahamas, is an approximately 100 kilometres (62 miles) long saltwater lagoon separating Great Abaco Island (known locally as the 'mainland') from a chain of barrier islands known as the Abaco Cays. Depths in the Sea of Abaco are generally a few metres, and shallow reefs and shoals can ...

  5. Holiday cheer on the high seas: Norwegian Gem to host ...

    www.aol.com/holiday-cheer-high-seas-norwegian...

    Traveling to Nassau, Bahamas, and back, passengers will be able to experience holiday cheer on the high seas, complete with cookie making, “carol-oke,” photo ops with network stars, and an ...

  6. Ready to take a ‘cat’ on the high seas? Luxury ... - AOL

    www.aol.com/ready-cat-high-seas-luxury-090000469...

    Say so long to seasickness. Imagine cruising to the Bahamas or Saint-Tropez without that stomach-churning feeling. A maritime adventure on a catamaran nearly guarantees a nauseous-free vacation.

  7. Tongue of the Ocean - Wikipedia

    en.wikipedia.org/wiki/Tongue_of_the_Ocean

    This channel and the Providence Channels are the two main branches of the Great Bahama Canyon, a submerged geological feature formed by erosion during periods of lower sea level. During their early history the Tongue of the Ocean and the Providence Channel were broad, relatively shallow basins flanked by growing carbonate banks .